Hydrological study of a basin for the evaluation of the potential of a Pico hydroelectric power station in a rural area
The goal of the study was to estimate the average monthly runoff from a basin for the development of a pico hydropower in a rural-mountainous area of the jungle (Satipo) on Peru. Due to the lack of hydrometeorological data in hilly and remote basins in Peru, a hydrological estimate is essential to d...
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Instituto Mexicano de Tecnologia del Agua
2022
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| author | Nieves Vilchez, Ines Aberli Castillo Infante, Hiram Joshua Carillo-Espinoza, Josué Isac Pampa Quispe, Noe Benjamin |
| author_browse | Carillo-Espinoza, Josué Isac Castillo Infante, Hiram Joshua Nieves Vilchez, Ines Aberli Pampa Quispe, Noe Benjamin |
| author_facet | Nieves Vilchez, Ines Aberli Castillo Infante, Hiram Joshua Carillo-Espinoza, Josué Isac Pampa Quispe, Noe Benjamin |
| author_sort | Nieves Vilchez, Ines Aberli |
| collection | Producción científica |
| description | The goal of the study was to estimate the average monthly runoff from a basin for the development of a pico hydropower in a rural-mountainous area of the jungle (Satipo) on Peru. Due to the lack of hydrometeorological data in hilly and remote basins in Peru, a hydrological estimate is essential to determine the hydroenergy potential in the study basin. First, the geomorphological parameters (shape and relief parameters) of the basin were determined and, subsequently, a precipitation analysis was made considering the data from 17 meteorological stations. To verify the homogeneity of the rainfall records, a consistency analysis was carried out using a double accumulation analysis. To estimate the flows of the study basin, in the absence of hydrometric information, the flow transposition method was used, in which the flows of the Ourohuari basin were transported. Likewise, it was verified that the geomorphological and hydrometeorological characteristics are similar, for this, a t-test was carried out for independent samples to verify the similarity in the annual precipitation between both basins. Finally, it can be concluded that the geomorphological characteristics and flow regular throughout the year in the Cashingari basin are favoring the development of a pico hydropower. |
| format | Article |
| id | oai:cris.upeu.edu.pe:20.500.15037/3162 |
| institution | UPeU |
| language | Spanish |
| publishDate | 2022 |
| publishDateRange | 2022 |
| publishDateSort | 2022 |
| publisher | Instituto Mexicano de Tecnologia del Agua |
| publisherStr | Instituto Mexicano de Tecnologia del Agua |
| record_format | dspace |
| spelling | oai:cris.upeu.edu.pe:20.500.15037/31622026-11-03T23:03:23ZHydrological study of a basin for the evaluation of the potential of a Pico hydroelectric power station in a rural areaEstudio hidrológico de una cuenca para la evaluación del potencial de una Pico central hidroeléctrica en una zona ruralNieves Vilchez, Ines AberliCastillo Infante, Hiram JoshuaCarillo-Espinoza, Josué IsacPampa Quispe, Noe Benjamincaudalprecipitaciónevaluación hidrológicapico centralThe goal of the study was to estimate the average monthly runoff from a basin for the development of a pico hydropower in a rural-mountainous area of the jungle (Satipo) on Peru. Due to the lack of hydrometeorological data in hilly and remote basins in Peru, a hydrological estimate is essential to determine the hydroenergy potential in the study basin. First, the geomorphological parameters (shape and relief parameters) of the basin were determined and, subsequently, a precipitation analysis was made considering the data from 17 meteorological stations. To verify the homogeneity of the rainfall records, a consistency analysis was carried out using a double accumulation analysis. To estimate the flows of the study basin, in the absence of hydrometric information, the flow transposition method was used, in which the flows of the Ourohuari basin were transported. Likewise, it was verified that the geomorphological and hydrometeorological characteristics are similar, for this, a t-test was carried out for independent samples to verify the similarity in the annual precipitation between both basins. Finally, it can be concluded that the geomorphological characteristics and flow regular throughout the year in the Cashingari basin are favoring the development of a pico hydropower.Article10.24850/j-tyca-2022-01-072-s2.0-85119897999https://hdl.handle.net/20.500.15037/3162esTecnología y Ciencias del AguaTecnologia y Ciencias del Agua0187-8336Instituto Mexicano de Tecnologia del Agua2022-01-012026-06-27T02:36:13Z2026-06-27T02:36:13Z |
| spellingShingle | caudal precipitación evaluación hidrológica pico central Nieves Vilchez, Ines Aberli Castillo Infante, Hiram Joshua Carillo-Espinoza, Josué Isac Pampa Quispe, Noe Benjamin Hydrological study of a basin for the evaluation of the potential of a Pico hydroelectric power station in a rural area |
| title | Hydrological study of a basin for the evaluation of the potential of a Pico hydroelectric power station in a rural area |
| title_full | Hydrological study of a basin for the evaluation of the potential of a Pico hydroelectric power station in a rural area |
| title_fullStr | Hydrological study of a basin for the evaluation of the potential of a Pico hydroelectric power station in a rural area |
| title_full_unstemmed | Hydrological study of a basin for the evaluation of the potential of a Pico hydroelectric power station in a rural area |
| title_short | Hydrological study of a basin for the evaluation of the potential of a Pico hydroelectric power station in a rural area |
| title_sort | hydrological study of a basin for the evaluation of the potential of a pico hydroelectric power station in a rural area |
| topic | caudal precipitación evaluación hidrológica pico central |
| topic_facet | caudal precipitación evaluación hidrológica pico central |
| url | https://hdl.handle.net/20.500.15037/3162 |
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